著者

菅原 努

出版者

大道学館出版部

雑誌

臨牀と研究 (ISSN:00214965)

巻号頁・発行日

vol.37, no.4, 1960-04

著者

菅原 努

出版者

日本臨床社

雑誌

日本臨床 (ISSN:00471852)

巻号頁・発行日

vol.32, no.1, pp.30-36, 1974-01

著者

菅原 努

出版者

医学書院

雑誌

綜合医学 (ISSN:03711803)

巻号頁・発行日

vol.18, no.9, 1961-09

著者

菅原 努

出版者

小西六写真工業

雑誌

さくらXレイ写真研究 (ISSN:03864537)

巻号頁・発行日

no.11, 1955-04

著者

菅原 努

出版者

金原出版

雑誌

臨床放射線 (ISSN:00099252)

巻号頁・発行日

vol.3, no.1, 1958-01

著者

近江一郎 著

出版者

五典書院

巻号頁・発行日

1940

著者

横溝 佐衣子 山本 信子 福田 満

出版者

The Japan Society of Home Economics

雑誌

一般社団法人日本家政学会研究発表要旨集

巻号頁・発行日

pp.134, 2004 (Released:2005-04-02)

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[目的]レトルト米や、新しい加工米が多種類開発されている。家事時間の軽減志向により、炊飯器も高温短時間で食味向上が期待されるIH式電気炊飯器や、玄米が炊ける多機能型も開発され、米の利用法や食べ方は多様化してきた。特に最近では、操作の簡便性と環境汚染の面から無洗米が普及し始めている。無洗米はBG米(糠で糠を除去する湿式処理米)が一般的であるが、さらに改良が進み、浸漬時間不要で炊き増え効果があるといわれる乾式無洗米が商品化された。そこで本実験ではこの無洗米に注目し、従来の無洗米(BG米)との食味の違いなどを検討することを目的とした。[方法]試料は「新無洗米(乾式処理)」と「従来のBG米(湿式処理)」の2種に、対照として2試料の無洗米に加工する前の「精白米」を用いた。炊飯操作は、メーカーのマニュアルに従った。即ち、精白米とBG米の加水量は、米重量の1.5倍で浸漬時間30分、新無洗米は1.6倍で浸漬時間は0分とした。官能検査は5段階評価の採点法、さらに吸水率、粒の大きさ、還元糖量、α化度、電子顕微鏡など食味にかかわる調理学的測定を行った。[結果]官能検査の総合評価では平均点の高い方から、精白米、新無洗米、BG米であった。香りについては2種の無洗米(BG米と新無洗米)が、精白米よりも評価点が高かった。しかし、色の評価は、どちらも精白米に比べて黄色いと評価された。無洗米同志の比較では還元糖量、α化度などには測定値に大きな違いはみられなかったが、粒の大きさでは新無洗米がやや膨らみが大きくなり、若干炊き増え効果がみられた。

著者

SATHER Jeremy A.

出版者

International Research Center for Japanese Studies

雑誌

Japan review : Journal of the International Research Center for Japanese Studies (ISSN:09150986)

巻号頁・発行日

vol.31, pp.25-40, 2017

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I have divided the translation of and commentary on Nan Taiheiki into two parts. In part one, I outlined the main concerns that influenced Ryōshun to write the text: the loyalty of the Imagawa to the ruling Ashikaga family, his frustration with Taiheiki (Chronicle of Great Peace), and his resentment toward Ashikaga Yoshimitsu. The overarching theme of Nan Taiheiki, then, is the protection of the Imagawa legacy. In part two, I continue my analysis of this theme through an examination of Ryōshun’s description of Hosokawa Kiyouji and his rebellion against the Ashikaga. Ryōshun’s father Norikuni proposed a plan to the shogun that would have sacrificed his son in an attempt to kill Kiyouji and nip his rebellion in the bud. I then examine the significance of the Kamakura outpost, its overlord the Kantō kubō, and his deputy the kanrei for both Kiyouji’s rebellion, which took place as a result of the strife surrounding the position of kanrei, and later, for Ryōshun’s participation in the Ōei Disturbance, which resulted from the discord between Kyoto and Kamakura. What Ryōshun likely perceived as similarities between his participation in the Ōei Disturbance and Kiyouji’s rebellion motivated him to include the Kiyouji episodes in Nan Taiheiki. Accordingly, Nan Taiheiki demonstrates, through Kiyouji, how easy it was to fall from grace, and, through the idealistic origins of the Kamakura outpost, just how far the Ashikaga had fallen under Yoshimitsu’s rule.

著者

室伏高信 著

出版者

日本評論社

巻号頁・発行日

1934

著者

塚本 孝

出版者

国立国会図書館調査及び立法考査局

雑誌

レファレンス (ISSN:00342912)

巻号頁・発行日

vol.44, no.3, pp.p31-56, 1994-03

著者

Yoshiko Yamasaki

出版者

日本国際問題研究所

雑誌

Japan Review (ISSN:24334456)

巻号頁・発行日

vol.2, no.3, pp.48-73, 2019-03-05

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This article was originally published as 山﨑佳子「韓国政府による竹島領有根拠の創作」竹島問題研究会『第 2 期「竹島問題に関する調査研究」最終報告書』島根県、2012年、61-78頁.

著者

Kenichi Kuwashima Nobuyuki Inamizu Nobuo Takahashi

出版者

Global Business Research Center

雑誌

Annals of Business Administrative Science (ISSN:13474464)

巻号頁・発行日

pp.0200621a, (Released:2020-08-03)

参考文献数

42

被引用文献数

5

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The concept of ambidexterity and particularly the concept of exploitation are ambiguous. March (1991), a study that became the theoretical basis for several research studies, asserted that exploitation has a trade-off relationship with exploration including innovation, and on the basis of this aspect, Levinthal and March (1993) proposed the myopia of learning. Nevertheless, Levinthal later modeled exploitation that can be called as innovation. Some argued that exploration and exploitation are bipolar on one axis, and some argued that they are two orthogonal axes. In this study, we proposed using Lévi-Strauss’ “bricolage” instead of “exploitation.” This bricolage is a concept of making do with the tools and materials at hand (performing innovation), and bricolage and exploration are used together with ambidexterity being the normal form. We examine this aspect by using Japan’s response to the current Coronavirus disease pandemic as an example.

著者

松隈 寿紀 宮久 三千年

出版者

日本鉱物科学会

雑誌

岩石鉱物鉱床学会誌 (ISSN:00214825)

巻号頁・発行日

vol.41, no.5, pp.173-180, 1957

著者

白水 晴雄 小川 留太郎 田中 信也 宮久 三千年

出版者

日本鉱物科学会

雑誌

岩石鉱物鉱床学会誌 (ISSN:00214825)

巻号頁・発行日

vol.46, no.6, pp.191-195, 1961

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Brucite from Sasaguri occurs as foliated or fibrous aggregates, associating with calcite and yellowish serpentine. H=2.5; S.G=2.475; ω=1.562, ε=1.581. Chemical analysis gives: SiO₂ 0.33, Al₂O₃ 0.08, Fe₂O₃ 1.69, MgO 64.81, MnO 1.10, H₂O(-)0.39, H₂O(+)31.38, total 99.78. X-ray powder data and D. T. A. curve are also given. The mineral seems to have been formed under hydrothermal condition.

著者

宮久 三千年 石橋 澄 足立 富男

出版者

日本鉱物科学会

雑誌

岩石鉱物鉱床学会誌 (ISSN:00214825)

巻号頁・発行日

vol.70, no.1, pp.25-29, 1975

被引用文献数

3

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Malayaite is found in the contact skarn zone of Toroku mine, Miyazaki Prefecture. The crystals are commonly granular to massive shape, but sometime crystals show platy to wedgelike aspect, which reach to 3cm in length. Color is white to greenish gray. Luster is resinous. Fluoluminescence of greenish yellow color is observed, when on ultraviolet ray. The refractive indices are <i>&alpha;</i>=1.764, <i>&beta;</i>=1.784-1.786, <i>&gamma;</i>=1.801 and 2V (+) 84-86.<br> Chemical formula calculated from the analysis is:<br> Ca_0.978Sn_0.980Ti_0.002 Si_1.002O_5.000<br>which is in good accord with Ca (Sn, Ti) SiO_5.000 of sphene-malayaite series.<br> Genetic considerations of ore-forming minerals, and problems of tin-mineral dressing are also discussed in this paper.

著者

宮久 三千年

出版者

資源地質学会

雑誌

鉱山地質 (ISSN:00265209)

巻号頁・発行日

vol.12, no.56, pp.317-323, 1962

被引用文献数

1

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The contact metasomatic and the vein-type ore deposits of the Shin-Kiura tin mine have been worked since old times for tin, silver, arsenic and copper. These are characterized by complex mineralization at a wide range of temperature related to the Tertiary granitic intrusion. Recently, lollingite-cassiterite-quartz-wollastonite vein-like deposits, containing native gold, native bismuth and tellurobismuthite, have been found in the Uriya-Kaneko adit of this mine.<BR>In this paper, mineragraphy of the Au-Te-Bi-As ore is presented, and genesis of the similar mineralizations in Japan is discussed.

著者

松隈 寿紀 宮久 三千年

出版者

日本鉱物科学会

雑誌

岩石鉱物鉱床学会誌 (ISSN:00214825)

巻号頁・発行日

vol.41, no.3, pp.89-97, 1957

著者

宮久 三千年 鹿島 愛彦

出版者

資源地質学会

雑誌

鉱山地質 (ISSN:00265209)

巻号頁・発行日

vol.17, no.84, pp.214-227, 1967

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Dolomite deposits of western Shikoku are distributed in some definite stratigraphic and geotectonic zone. They are classified into the following group.<BR>1) Siliceous dolomite deposits of the northern zone of upper Carboniferous in age. These deposits are associated with red tuff, red chert, and other clastic sediments of volcanic materials.<BR>2) Some workable dolomite deposits of the southern zone of lower Triassic Uonashi formation, independent of volcanic activities.<BR>Chief factors of the formation of dolomite are temperature, pH, Eh and concentration of Mg-ion in the sea-water of geosynclinal basin. These factors are related to some paleogeographical environments, such as submarine volcanism (Northern zone) and development of shallow sedimentary basin of nearshore line (Southern zone).<BR>Chemical compositions of mineral dolomites, mechanism of dolomitization, deformation and recrystallization of ores, and relation of dolomite bed to other submarine sedimentary ore deposits are also discussed in this paper.

著者

宮久 三千年 原田 進造 石橋 澄 渋谷 五郎 本村 慶信

出版者

資源地質学会

雑誌

鉱山地質 (ISSN:00265209)

巻号頁・発行日

vol.25, no.133, pp.347-357, 1975

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In this paper, the paragenesis of minerals in the Hoei mine is presented with some remarks on the mineralogical properties of kutnahorite.<BR>The Ichigo (no.1) ore body of the Hoei mine is a massive deposit of Sn, Zn and iron sulfide formed by replacement of the Silurian limestone bed. From this ore body, there have been found various kinds of ore and gangue minerals such as: garnet, clinopyroxene, axinite, tourmaline, vesuvianite, quartz, pyrrhotite, chalcopyrite, arsenopyrite, pyrite, marcasite, sphalerite, galena, native bismuth, herzenbergite, franckeite, jamesonite, cassiterite, stannite, malayaite, fluorite, sericite and carbonate minerals. The species of carbonate minerals are ferromanganoan dolomite, magnesian kutnahorite, kutnahorite, calcian rhodochrosite, ferroan magnesite and manganoan calcite, and they have been crystallized at the later stage of mineralization in this mine.<BR>The kutnahorite in this mine is white, yellow or pinkish in color, and platy or leaf-like in external shape, reaching to 5 cm in maximum length. Its specific gravity ranges from 2.98 to 3.18 by picnometer method. Optically negative, and some examples of refractive indices are &omega;=1.717-1.731, &epsilon;=1.524-1.529. Unit cell constants, a<SUB>0</SUB> = 4.861-4.869 &Aring;, c<SUB>0</SUB>=16.24-16.37 &Aring;. The range of chemical composition of kutnahorite is fairly wide, as shown in Table 4 and 5.<BR>Judging from the mode of occurence, microscopic observations and the compositional changes detected by EPMA, the crystallization sequence of the carbonate minerals is suggested as follows : dolomite-ferromanganoan dolomite-magnesian kutnahorite-kutnahorite-calcian rhodochrosite-manganoan calcite.

著者

宮久 三千年 野田 雅之

出版者

日本鉱物科学会

雑誌

鉱物学雜誌 (ISSN:04541146)

巻号頁・発行日

vol.6, no.6, pp.349-360_2, 1964